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  • Continental Margin: Understanding the Slope and Rise
    The continental shelf slope and rise combine to form the continental margin.

    Here's a breakdown:

    * Continental Shelf: This is the gently sloping, submerged area extending outward from the shoreline. It's relatively shallow and is often where you'll find rich marine life and important fishing grounds.

    * Continental Slope: This is a steeper incline that marks the transition between the shelf and the deep ocean floor. It's characterized by canyons and submarine channels, often formed by sediment flows.

    * Continental Rise: This is a gentler slope at the base of the continental slope. It's formed by the accumulation of sediment carried down from the shelf and slope by turbidity currents.

    Together, these three components form the continental margin, which is essentially the submerged edge of a continent.

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